Supercell thunderstorm produces giant hail and 100 mph winds in South Dakota
1-minute Mesoscale Domain Sector GOES-16 (GOES-East) “Red” Visible (0.64 µm) images (above) showed a supercell thunderstorm that produced a tornado, hail as large as 5.00 inches in diameter and wind gusts to 100 mph (SPC Storm Reports | NWS Aberdeen summary) in central South Dakota during the late afternoon and early evening hours on 18 July 2023. Several pulses of overshooting tops were evident in the visible imagery, an indicator of vigorous thunderstorm updrafts. It bears mention that 10 minutes prior to the 100 mph wind gust (at 0115 UTC), there were reports of semi trucks overturned by strong winds along Interstate 90 (in eastern Lyman County at 0105 UTC). The peak wind gust at nearby Chamberlain (K9V9) was 53 knots (61 mph) at 0122 UTC.In the corresponding 1-minute GOES-16 “Clean” Infrared Window (10.3 µm) images (below), the coldest thunderstorm overshooting tops exhibited infrared brightness temperatures around -70ºC (brighter white pixels embedded within dark black regions).
A closer view of Infrared imagery at 2347 UTC (below) revealed that a report of 4.50″ diameter hail occurred within a cluster of 2 other reports of 2.75″ diameter hail just southwest of Pierre (KPIR) — in fact, with further evidence the size of that largest hail was later upgraded to 5.00 inches (which was a record hail size for Hughes County in South Dakota: media report). A cursor sample of GOES-16 infrared (10.3 µm) brightness temperature, Cloud Top Temperature and Cloud Top Height derived products at 0021 UTC (above) displayed values of -72.61ºC, -77.64ºC and 47031.21 feet, respectively — these Cloud Top Temperature and Cloud Top Height values were similar to those of a Most Unstable (MU) air parcel’s Maximum Parcel Level (MPL), calculated using 0000 UTC rawinsonde data (source) from Aberdeen SD (below). 1-minute GOES-16 Visible images with an overlay of GLM Flash Extent Density (below) showed modest lightning activity with this thunderstorm, with a number of minor lightning jumps during that time period. In a larger-scale view of GOES-16 Infrared and Visible images (below), the signature of an Above-Anvil Cirrus Plume (reference | VISIT training) was evident in the Visible imagery (but was more subtle in the Infrared imagery). The supercell thunderstorm developed within a corridor of instability and moisture that existed in the warm sector between a cold front and a warm front (surface analyses) — as seen in GOES-16 Convective Available Potential Energy (CAPE), Lifted Index and Total Precipitable Water derived products (below). CAPE values were around 1900 J/kg, Lifted Index values were around -7ºC and Total Precipitable Water values were around 1.6 inches.